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DOI10.1007/s11629-020-6240-y
Characteristics of the active-layer under the China-Russia Crude Oil pipeline
Serban, Mihaela; Li Guo-yu; Serban, Raul-David; Wang Fei; Fedorov, Alexander; Vera, Samsonova; Cao Ya-peng; Chen Peng-chao; Wang Wei
通讯作者Li, GY (通讯作者),Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soils Engn, Lanzhou 730000, Peoples R China. ; Li, GY (通讯作者),Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Da Xinganling Observat & Res Stn Frozen Ground En, Jiagedaqi 165000, Peoples R China.
发表日期2021
ISSN1672-6316
EISSN1993-0321
起始页码323
结束页码337
卷号18期号:2
英文摘要Active layer is a key component for permafrost environment studies as many subsurface biological, biogeochemical, ecological, and pedogenic activities prevail in this layer. This study focuses on active layer temperature monitoring in an area with sporadic permafrost at two adjacent sites along China-Russia Crude Oil Pipeline (CRCOP), North-East China. Site T1 is located in disturbed ground on the right-of-way (on-ROW) 2 m away from the center of the oil pipeline. T2 is located in a natural and undisturbed site, around 16.6 m off-ROW. Our objective was to study seasonal variability of the active layer depth and thermal regime from October 2017 to September 2018. The monitoring sites consist of soil temperature probes arranged in a vertical array at different depths at both sites. The following parameters were computed: number of isothermal days (ID), freezing days (FD), thawing days (TD), freezing degree days (FDD), thawing degree days (TDD), number of freeze-thaw days (FTD). The mean air temperature in the monitoring period reached - 3.2 degrees C. The temperature profile indicates that the maximum active layer thickness observed during the study period was 10 m at T1 and 2 m at T2. The majority of the soil temperatures were above or close to 0 degrees C, resulting in great values of TDD, especially in the first 4 m depth. TDD for T1 were predominant and ranged between 600-1160 degrees C center dot days (0-4 m depth) reflecting the influence of oil temperature from the pipeline. In T2 borehole FDD were predominant for all the soil layer depths resulting in less permafrost degradation. This comparison emphasizes the significant influence of vegetation removal and the dispersed heat from the pipeline on the active layer thickness.
关键词PENINSULA LIVINGSTON ISLANDGROUND SURFACE TEMPERATURESQINGHAI-TIBET PLATEAUTHERMAL REGIMEFOUNDATION SOILSPERMAFROST AREASENGINEERING GEOLOGYMARITIME ANTARCTICANORTHEASTERN CHINADEGRADATION
英文关键词Soil thermal regime; Permafrost; China-Russia Crude Oil Pipeline; Active layer
语种英语
WOS研究方向Environmental Sciences & Ecology
WOS类目Environmental Sciences
WOS记录号WOS:000608965700002
来源期刊JOURNAL OF MOUNTAIN SCIENCE
来源机构中国科学院西北生态环境资源研究院
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/253915
作者单位[Serban, Mihaela; Li Guo-yu; Serban, Raul-David; Wang Fei; Cao Ya-peng] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soils Engn, Lanzhou 730000, Peoples R China; [Li Guo-yu] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Da Xinganling Observat & Res Stn Frozen Ground En, Jiagedaqi 165000, Peoples R China; [Wang Fei; Cao Ya-peng] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Fedorov, Alexander; Vera, Samsonova] SB RAS, Melnikov Permafrost Inst, Yakutsk 677010, Russia; [Chen Peng-chao] PetroChina Pipeline Co, Langfang 065000, Peoples R China; [Wang Wei] PetroChina Pipeline Co, Jiagedaqi Oil & Gas Transmiss Sub Co, Jiagedaqi 165000, Peoples R China
推荐引用方式
GB/T 7714
Serban, Mihaela,Li Guo-yu,Serban, Raul-David,et al. Characteristics of the active-layer under the China-Russia Crude Oil pipeline[J]. 中国科学院西北生态环境资源研究院,2021,18(2).
APA Serban, Mihaela.,Li Guo-yu.,Serban, Raul-David.,Wang Fei.,Fedorov, Alexander.,...&Wang Wei.(2021).Characteristics of the active-layer under the China-Russia Crude Oil pipeline.JOURNAL OF MOUNTAIN SCIENCE,18(2).
MLA Serban, Mihaela,et al."Characteristics of the active-layer under the China-Russia Crude Oil pipeline".JOURNAL OF MOUNTAIN SCIENCE 18.2(2021).
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